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Surface and ground-water origins and interactions and vegetation distributions in riverine and reservoir-fringe systems: A case study in support of reservoir management efforts.

机译:河流和水库边缘系统中的地表水和地下水起源以及相互作用和植被分布:以支持水库管理工作为例的研究。

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This dissertation explores surface and ground-water origins and interaction and associated vegetation in riverine and reservoir-fringe systems. The overall objective of this effort is to develop concepts and tools for the planning, implementation, and monitoring stages of river and reservoir management efforts. This study was conducted where Little Stony Creek flows into East Park Reservoir on the east front of the Coast Range, northern California.; Turnover in the local ground-water flow system is rapid indicating that local shallow ground water is dependent upon recent recharge. Little Stony Creek is the more prominent source of local shallow ground water in the wet season, while Franciscan Complex ground water is the more prominent source of local shallow ground water in the dry season.; The flow paths of local shallow ground water are controlled by stream discharge, regional ground-water discharge, and reservoir stage. A ground-water backwater effect caused by the imposed reservoir head extends up valley and supports longer-lived stream discharge and shallower ground water on the delta. During the wet season, changes in stream stage are propagated rapidly across the local ground-water flow system but are slightly attenuated by distance from the channel. During the dry season, stream stage and head on the upper and lower reaches decline steadily and show diurnal fluctuations consistent with evapotranspiration and show abrupt variations likely due to ground-water pumping and rare summer storm events. The effects of changes in stream stage and ground-water pumping are strongly attenuated by the ground-water backwater effect on the delta.; A linked ground-water and vegetation model is developed and used to simulate shallow ground water and vegetation under varying reservoir operations. A numerical ground-water model is constructed, calibrated, and validated and coupled to a vegetation model based on an application of Bayes' Theorem. Four scenarios are simulated: Existing Condition, Existing Condition with Late Drawdown, Full Drawdown, and Full Pool. Compared to the Existing Condition scenario, modeled vegetation distributions do not change under the Existing Condition with Late Drawdown scenario, a xeric herbaceous community type is greatly expanded under the Full Drawdown scenario, and mesic herbaceous, scrub-shrub, and forested community types are greatly expanded under the Full Pool scenario.
机译:本文探讨了河流和水库边缘系统中地表水和地下水的起源,相互作用以及相关的植被。这项工作的总体目标是为河流和水库管理工作的规划,实施和监测阶段开发概念和工具。这项研究是在Little Stony Creek流入加利福尼亚北部海岸山脉东线东公园水库的地方进行的。当地地下水流系统的周转迅速,表明当地浅层地下水取决于最近的补给。 ;小石溪是雨季当地浅层地下水的最主要来源,而方济各会综合体地下水是旱季当地浅层地下水的最主要来源。局部浅层地下水的流路由水流排放,区域地下水排放和水库蓄水阶段控制。由强加的水库水头引起的地下水回水效应延伸到山谷上方,并支持三角洲上寿命更长的河流排放和较浅的地下水。在雨季,河段的变化会迅速传播到整个当地的地下水流系统中,但随着距河道的距离而略微减弱。在干旱季节,上游和下游的水位和水头稳步下降,并显示出与蒸散量一致的昼夜波动,并可能由于地下水抽水和罕见的夏季风暴事件而出现突变。三角洲的地下水回水效应大大减弱了水位变化和地下水泵送的影响。建立了地下水与植被的链接模型,并使用该模型来模拟在变化的水库运行条件下的浅层地下水和植被。基于贝叶斯定理的应用,构造,校准和验证了数值地下水模型,并将其与植被模型耦合。模拟了四个方案:现有条件,具有延迟提款的现有条件,完全提款和完整池。与“现有条件”方案相比,在“存在延迟提现的现有条件”情况下,模拟的植被分布不会发生变化,在“完全提用”情况下,旱生草本群落类型大大扩展,而中生草本,灌木丛和森林群落类型则大大增加在全池方案下扩展。

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